Evolution and Facies Architecture of A Himalayan Cretaceous Forearc Basin

Authors

  • G. Einsele et al.

DOI:

https://doi.org/10.51835/bsed.1998.7.1.289

Abstract

The mid-Cretaceous to Eocene flysch deposits of the Xigaze forearc basin in southern Tibet were investigated in a 120 km segment along the Indus Yarlung suture zone. The basin evolved south of the magnetic arc (Gangdise belt) of the Lhasa block on top of trapped oceanic or transitional crust.

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Published

2021-08-07

How to Cite

Einsele et al., G. (2021). Evolution and Facies Architecture of A Himalayan Cretaceous Forearc Basin. Berita Sedimentologi, 7(1), 5–6. https://doi.org/10.51835/bsed.1998.7.1.289

Issue

Vol. 7 No. 1 (1998)

Section

Articles

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